PROSPERIDAD J. ABONETE JULY 3, 2003 Understanding Climate Change.
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Transcript of PROSPERIDAD J. ABONETE JULY 3, 2003 Understanding Climate Change.
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PROSPERIDAD J. ABONETEJULY 3, 2003
Understanding Climate Change
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Outline
Climate Change and Global Warming Definition Causes
The Greenhouse EffectEvidence of Climate ChangeEffects of Global Warming
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Climate change
Long-term change in the average weather patterns over a specific period, over a significant period of time
The Earth's climate has always varied, so the term climate change is now generally used to describe the changes caused by human activity - specifically, greenhouse emissions which build up in the atmosphere and trap heat.
Global Warming, increase in the average temperature of the atmosphere, oceans, and landmasses of Earth
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Causes of Climate Change
Solar variationOrbital variationPlate tectonicsVolcanic actionThermohaline circulationHuman influences
Measurements at the Earth's surface show that average temperatures have risen by some 0.4C since the 1970s. Scientists are confident this change can be blamed on human emissions because the increase is too big to be explained by natural causes.
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Although natural factors such as changes in the sun and large volcanic eruptions are known to have warmed and cooled the planet in the past, these effects are not powerful enough to explain the rapid warming seen recently. Only an increased greenhouse effect caused by higher amounts of heat-trapping gases in the atmosphere can explain it.
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The Greenhouse Effect
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Greenhouse Gases
Occur naturallyConcentrations determined by natural factorsNaturally-occurring GHGs:
Water vapor Methane (CH4) Nitrous oxide (N20) Carbon dioxide (CO2)
Not naturally occurring: Halocarbons – e.g CFCs Artificial/human-made; products from chemical
industry
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Enhanced Greenhouse Effect
Today, concentrations of naturally occurring GHGs, e.g. CO2, are enhanced by human action
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Summary of Principal Greenhouse Gases
GHG CO2 CH4 CFC-11 CFC-12 N2O
Atmospheric concentration
Late 18th century
280 ppm 0.7 ppm 0 0 288 ppb
2001 371 ppm 1.75 ppm 252 ppt 480 ppt 315 ppb
Atmospheric lifetime (yrs)
50-200 12 45 130 114
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Carbon Cycle
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The current concentrations of greenhouse gases
IPCC WG1 SPM, 2007
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13
Carbon dioxide and temperature last 420, 000 years
100
150
200
250
300
350
0100,000200,000300,000400,000years before present
CO
2 (p
pm)
-10
0
10
20
tem
pera
ture
(oC
)
Source: Jones, 2002
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Global Surface Temperature (IPCC, 2007)
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Intergovernmental Panel on Climate Change (IPCC)
International scientific guidanceEstablished in 1988 by WMO & UNEPTasks:
Assess the scientific information related to the various components of the CC issue, such as…, as well as the science needed to assess environmental and socio-economic consequences
Formulate realistic response strategies for the management of CC issues
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IPCC 2007 Report
The understanding of anthropogenic warming and cooling influences on climate has improved …, leading to very high confidence that the globally averaged net effect of human activities since 1750 has been one of warming….
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Warming of the climate system is unequivocal…. Increases in global average air and ocean temperatures Widespread melting of snow and ice Rising global mean sea level
Anthropogenic warming and sea level rise would continue for centuries due to timescales associated with climate processes and feedbacks, even if GHG concentrations were to be stabilized.
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Effects of Global Warming
Weather Sea levelsAgricultureAnimals &
PlantsHuman Health
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Forests
Climate interrelated with biology/ecologyRising CO2 levels – increased global temperatureCarbon sequestration by forestsforest vegetation accounts for 80% of above-
ground C; forest soils capture 40% C of soil Cforests both C source and sinkeven 1oC change in air T sustained over time is
likely to affect growth and regeneration patterns of many forest species
1/3 of global forests will experience major changes